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a:5:{s:8:"template";s:46130:"<!DOCTYPE html>
<html lang="en">

   <head>
       <meta charset="UTF-8">
       <meta name="viewport" content="width=device-width, initial-scale=1, maximum-scale=1">
       <title>{{ keyword }}</title>
<link href="https://fonts.googleapis.com/css?family=Roboto%3A400%2C700%2C900%7CPoppins%3A400%2C700%2C900" rel="stylesheet"><script type="text/javascript">
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		<style type="text/css">
img.wp-smiley,
img.emoji {
	display: inline !important;
	border: none !important;
	box-shadow: none !important;
	height: 1em !important;
	width: 1em !important;
	margin: 0 .07em !important;
	vertical-align: -0.1em !important;
	background: none !important;
	padding: 0 !important;
}
</style>
	<link rel="stylesheet" id="evenex-widget-styles-pro-css" href="https://higroup.coding.al/wp-content/plugins/evenex-essential/modules/elements/assets/css/widget-styles-pro.css?ver=1.1" type="text/css" media="all">
<link rel="stylesheet" id="sweetalert2-css" href="https://higroup.coding.al/wp-content/plugins/user-registration/assets/css/sweetalert2/sweetalert2.min.css?ver=8.17.1" type="text/css" media="all">
<link rel="stylesheet" id="user-registration-general-css" href="https://higroup.coding.al/wp-content/plugins/user-registration/assets/css/user-registration.css?ver=1.9.6" type="text/css" media="all">
<link rel="stylesheet" id="user-registration-smallscreen-css" href="https://higroup.coding.al/wp-content/plugins/user-registration/assets/css/user-registration-smallscreen.css?ver=1.9.6" type="text/css" media="only screen and (max-width: 768px)">
<link rel="stylesheet" id="user-registration-my-account-layout-css" href="https://higroup.coding.al/wp-content/plugins/user-registration/assets/css/my-account-layout.css?ver=1.9.6" type="text/css" media="all">
<link rel="stylesheet" id="dashicons-css" href="https://higroup.coding.al/wp-includes/css/dashicons.min.css?ver=5.8.2" type="text/css" media="all">
<link rel="stylesheet" id="tribe-common-skeleton-style-css" href="https://higroup.coding.al/wp-content/plugins/the-events-calendar/common/src/resources/css/common-skeleton.min.css?ver=4.13.0.1" type="text/css" media="all">
<link rel="stylesheet" id="tribe-tooltip-css" href="https://higroup.coding.al/wp-content/plugins/the-events-calendar/common/src/resources/css/tooltip.min.css?ver=4.13.0.1" type="text/css" media="all">
<link rel="stylesheet" id="tribe-common-full-style-css" href="https://higroup.coding.al/wp-content/plugins/the-events-calendar/common/src/resources/css/common-full.min.css?ver=4.13.0.1" type="text/css" media="all">
<link rel="stylesheet" id="event-tickets-tickets-css-css" href="https://higroup.coding.al/wp-content/plugins/event-tickets/src/resources/css/tickets-v1.min.css?ver=5.1.2.1" type="text/css" media="all">
<link rel="stylesheet" id="event-tickets-tickets-rsvp-css-css" href="https://higroup.coding.al/wp-content/plugins/event-tickets/src/resources/css/rsvp-v1.min.css?ver=5.1.2.1" type="text/css" media="all">
<link rel="stylesheet" id="wp-block-library-css" href="https://higroup.coding.al/wp-includes/css/dist/block-library/style.min.css?ver=5.8.2" type="text/css" media="all">
<style id="wp-block-library-theme-inline-css" type="text/css">
#start-resizable-editor-section{display:none}.wp-block-audio figcaption{color:#555;font-size:13px;text-align:center}.is-dark-theme .wp-block-audio figcaption{color:hsla(0,0%,100%,.65)}.wp-block-code{font-family:Menlo,Consolas,monaco,monospace;color:#1e1e1e;padding:.8em 1em;border:1px solid #ddd;border-radius:4px}.wp-block-embed figcaption{color:#555;font-size:13px;text-align:center}.is-dark-theme .wp-block-embed figcaption{color:hsla(0,0%,100%,.65)}.blocks-gallery-caption{color:#555;font-size:13px;text-align:center}.is-dark-theme .blocks-gallery-caption{color:hsla(0,0%,100%,.65)}.wp-block-image figcaption{color:#555;font-size:13px;text-align:center}.is-dark-theme .wp-block-image figcaption{color:hsla(0,0%,100%,.65)}.wp-block-pullquote{border-top:4px solid;border-bottom:4px solid;margin-bottom:1.75em;color:currentColor}.wp-block-pullquote__citation,.wp-block-pullquote cite,.wp-block-pullquote footer{color:currentColor;text-transform:uppercase;font-size:.8125em;font-style:normal}.wp-block-quote{border-left:.25em solid;margin:0 0 1.75em;padding-left:1em}.wp-block-quote cite,.wp-block-quote footer{color:currentColor;font-size:.8125em;position:relative;font-style:normal}.wp-block-quote.has-text-align-right{border-left:none;border-right:.25em solid;padding-left:0;padding-right:1em}.wp-block-quote.has-text-align-center{border:none;padding-left:0}.wp-block-quote.is-large,.wp-block-quote.is-style-large{border:none}.wp-block-search .wp-block-search__label{font-weight:700}.wp-block-group.has-background{padding:1.25em 2.375em;margin-top:0;margin-bottom:0}.wp-block-separator{border:none;border-bottom:2px solid;margin-left:auto;margin-right:auto;opacity:.4}.wp-block-separator:not(.is-style-wide):not(.is-style-dots){width:100px}.wp-block-separator.has-background:not(.is-style-dots){border-bottom:none;height:1px}.wp-block-separator.has-background:not(.is-style-wide):not(.is-style-dots){height:2px}.wp-block-table thead{border-bottom:3px solid}.wp-block-table tfoot{border-top:3px solid}.wp-block-table td,.wp-block-table th{padding:.5em;border:1px solid;word-break:normal}.wp-block-table figcaption{color:#555;font-size:13px;text-align:center}.is-dark-theme .wp-block-table figcaption{color:hsla(0,0%,100%,.65)}.wp-block-video figcaption{color:#555;font-size:13px;text-align:center}.is-dark-theme .wp-block-video figcaption{color:hsla(0,0%,100%,.65)}.wp-block-template-part.has-background{padding:1.25em 2.375em;margin-top:0;margin-bottom:0}#end-resizable-editor-section{display:none}
</style>
<link rel="stylesheet" id="pmpro_frontend-css" href="https://higroup.coding.al/wp-content/plugins/paid-memberships-pro/css/frontend.css?ver=2.5.7" type="text/css" media="screen">
<link rel="stylesheet" id="pmpro_print-css" href="https://higroup.coding.al/wp-content/plugins/paid-memberships-pro/css/print.css?ver=2.5.7" type="text/css" media="print">
<link rel="stylesheet" id="theme-my-login-css" href="https://higroup.coding.al/wp-content/plugins/theme-my-login/assets/styles/theme-my-login.min.css?ver=7.1.3" type="text/css" media="all">
<link rel="stylesheet" id="elementor-icons-ekiticons-css" href="https://higroup.coding.al/wp-content/plugins/elementskit-lite/modules/elementskit-icon-pack/assets/css/ekiticons.css?ver=2.5.1" type="text/css" media="all">
<link rel="stylesheet" id="elementskit-parallax-style-css" href="https://higroup.coding.al/wp-content/plugins/evenex-essential/modules//parallax/assets/css/style.css?ver=1.5.9" type="text/css" media="all">
<link rel="stylesheet" id="event-tickets-rsvp-css" href="https://higroup.coding.al/wp-content/plugins/event-tickets/src/resources/css/rsvp.min.css?ver=5.1.2.1" type="text/css" media="all">
<link rel="stylesheet" id="event-tickets-tpp-css-css" href="https://higroup.coding.al/wp-content/plugins/event-tickets/src/resources/css/tpp.min.css?ver=5.1.2.1" type="text/css" media="all">
<link rel="stylesheet" id="fonts-css" href="https://fonts.googleapis.com/css?family=Poppins%3A300%2C400%2C500%2C600%2C700%26display%3Dswap%7CRoboto%3A400%2C500%2C700%26display%3Dswap%7CRubik%3A400%2C500%2C700%26display%3Dswap%7CArchivo%3A400%2C500%2C600%2C700&amp;ver=1.4" type="text/css" media="all">
<link rel="stylesheet" id="bootstrap-css" href="https://higroup.coding.al/wp-content/themes/evenex/assets/css/bootstrap.min.css?ver=1.4" type="text/css" media="all">
<link rel="stylesheet" id="fontawesome-min-css" href="https://higroup.coding.al/wp-content/themes/evenex/assets/css/fontawesome.min.css?ver=1.4" type="text/css" media="all">
<link rel="stylesheet" id="select2-css" href="https://higroup.coding.al/wp-content/plugins/user-registration/assets/css/select2.css?ver=1.9.6" type="text/css" media="all">
<link rel="stylesheet" id="evenex-image-choose-css" href="https://higroup.coding.al/wp-content/themes/evenex/assets/css/image-choose-control.css?ver=1.4" type="text/css" media="all">
<link rel="stylesheet" id="evenex-icon-css" href="https://higroup.coding.al/wp-content/themes/evenex/assets/css/iconfont.css?ver=1.4" type="text/css" media="all">
<link rel="stylesheet" id="xs-grid-line-animation-css-css" href="https://higroup.coding.al/wp-content/themes/evenex/assets/css/grid-line-parallax.css?ver=1.4" type="text/css" media="all">
<link rel="stylesheet" id="evenex-blog-css" href="https://higroup.coding.al/wp-content/themes/evenex/assets/css/blog.css?ver=1.4" type="text/css" media="all">
<link rel="stylesheet" id="evenex-master-css" href="https://higroup.coding.al/wp-content/themes/evenex/assets/css/master.css?ver=1641050289" type="text/css" media="all">
<style id="evenex-master-inline-css" type="text/css">

      h1{
         font-family: Poppins, sans-serif;color:#101010;font-size:36px;
      }
      h2,
      .post .entry-header .entry-title,
      .search .page .entry-header .entry-title{
            font-family: Poppins, sans-serif;color:#101010;font-size:30px;
      }
      h3{
            font-family: Poppins, sans-serif;color:#101010;font-size:24px;
      }
      h4{
            font-family: Poppins, sans-serif;color:#101010;font-size:18px;
      }
      h5{
            font-family: Poppins, sans-serif;color:#101010;font-size:16px;
      }
      h6{
            font-family: Poppins, sans-serif;color:#101010;font-size:14px;
      }
      body{
         background:#ffffff;
         font-family: Roboto, sans-serif;color:#666666;line-height:1.625;font-size:16px;
      }
      .logo-area .site-title a , .logo-area .site-desc{
         color:#ec962d;
      }

      .post .entry-header .entry-title a:hover,
      .sidebar ul li a:hover, .xs-footer-section ul li a:hover,
      .post-meta a:hover,
      .header .navbar-light .navbar-nav li a:hover {
         color:  #ec962d;
      }
      .tag-lists a:hover, .tagcloud a:hover,
      .sticky.post .meta-featured-post,
      .widget-title:before,
      .xs-custom-widget > h5:before,
      .block-title.title-border .title-bg,
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      .header .navbar-light .navbar-nav>li.active>a:before,
      .main-slider .owl-prev.disabled,
      .owl-dots:before,
      .featured-tab-item .nav-tabs .nav-link.active:before,
      .owl-theme .owl-dots .owl-dot.active span,
      .ts-footer .widget-title:before,
      .main-slider .owl-next:hover, .main-slider .owl-prev:hover,
      .sidebar .widget.widget_search .input-group-btn, .xs-footer-section .widget.widget_search .input-group-btn,
      .xs-search-group .search-button,
      .banner-solid,
      .pagination li.active a,
      .wp-block-button:not(.is-style-outline) .wp-block-button__link,
      .wp-block-button .wp-block-button__link:not(.has-background),
      .wp-block-file .wp-block-file__button,
      .back_to_top > a,
      .post .meta-featured-post::after {
         background:#ec962d;
      }
      .post .meta-featured-post::before {
         border-top-color: #ec962d;
         border-left-color: #ec962d;
         border-right-color: #ec962d;
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      .xs-search-group .search-button:hover,
      .pagination li.active a:hover,
      .wp-block-button:not(.is-style-outline) .wp-block-button__link:hover,
      .wp-block-file .wp-block-file__button:hover {
         background:#ff7c49;
      }
      .header-btn {
         background: linear-gradient(90deg,#ec962d 0,#ff7c49 100%);
      }
      .header-btn::before {
         box-shadow: 0 15px 25px 0 #ec962d;
      }
      .is-style-outline .wp-block-button__link:hover,
      .wp-block-button.is-style-outline .wp-block-button__link:active:not(.has-text-color):hover,
      .wp-block-button.is-style-outline .wp-block-button__link:focus:not(.has-text-color):hover,
      .wp-block-button.is-style-outline .wp-block-button__link:not(.has-text-color):hover,
      .breadcrumb>li a:hover {
         color: #ff7c49;
      }
      .wp-block-button.is-style-outline .wp-block-button__link:active:not(.has-text-color),
      .wp-block-button.is-style-outline .wp-block-button__link:focus:not(.has-text-color),
      .wp-block-button.is-style-outline .wp-block-button__link:not(.has-text-color),
      .navbar-nav .nav-link:hover,
      .dropdown-item.active,
      .dropdown-item:active,
      .navbar-nav .dropdown-menu li:hover>a,
      .xs-recent-post-widget .widget-post .entry-title>a:hover {
         color: #ec962d;
      }
      .tag-lists a:hover, .tagcloud a:hover,
      .owl-theme .owl-dots .owl-dot.active span{
         border-color: #ec962d;
      }
      .block-title.title-border .title-bg::after{
         border-left-color: #ec962d;
      }
      .block-title.title-border{
         border-bottom-color: #ec962d;
      }

      .topbar .top-nav li a:hover,
      .comments-list .comment-author a:hover,
      .comments-list .comment-reply-link:hover,
      .post-title a:hover,
      .copyright-area a:hover,
      .ts-footer .widget ul li a:hover,
      .featured-tab-item .nav-tabs .nav-link.active .tab-head>span.tab-text-title,
      .social-links li a:hover,
      .comment-author cite a:hover {
         color:#ec962d;
      }
      .xs-footer-section{
         background-color:   #FFF;
      }
      .btn-primary {
         background: linear-gradient(90deg, #ec962d 0, #ff7c49 100%);
      }
      .sidebar .widget .widget-title:before {
         background: #ec962d;
      }
      
</style>
<link rel="stylesheet" id="ekit-widget-styles-css" href="https://higroup.coding.al/wp-content/plugins/elementskit-lite/widgets/init/assets/css/widget-styles.css?ver=2.5.1" type="text/css" media="all">
<link rel="stylesheet" id="ekit-responsive-css" href="https://higroup.coding.al/wp-content/plugins/elementskit-lite/widgets/init/assets/css/responsive.css?ver=2.5.1" type="text/css" media="all">
<script type="text/javascript" src="https://higroup.coding.al/wp-includes/js/jquery/jquery.min.js?ver=3.6.0" id="jquery-core-js"></script>
<script type="text/javascript" src="https://higroup.coding.al/wp-includes/js/jquery/jquery-migrate.min.js?ver=3.3.2" id="jquery-migrate-js"></script>
<script src="https://higroup.coding.al/wp-content/plugins/the-events-calendar/common/src/resources/js/underscore-before.js"></script>
<script type="text/javascript" src="https://higroup.coding.al/wp-includes/js/underscore.min.js?ver=1.13.1" id="underscore-js"></script>
<script src="https://higroup.coding.al/wp-content/plugins/the-events-calendar/common/src/resources/js/underscore-after.js"></script>
<script type="text/javascript" src="https://higroup.coding.al/wp-includes/js/wp-util.js?ver=5.8.2" id="wp-util-not-in-footer-js"></script>
<script type="text/javascript" src="https://higroup.coding.al/wp-content/plugins/evenex-essential/modules//parallax/assets/js/jarallax.js?ver=1.5.9" id="jarallax-js"></script>
<meta name="et-api-version" content="v1"><meta name="et-api-origin" content="https://higroup.coding.al"><link rel="https://theeventscalendar.com/" href="https://higroup.coding.al/index.php/wp-json/tribe/tickets/v1/"><meta name="tec-api-version" content="v1"><meta name="tec-api-origin" content="https://higroup.coding.al"><link rel="https://theeventscalendar.com/" href="https://higroup.coding.al/index.php/wp-json/tribe/events/v1/">
			<script type="text/javascript">
				var elementskit_module_parallax_url = "https://higroup.coding.al/wp-content/plugins/evenex-essential/modules//parallax/"
			</script>
		<meta name="msapplication-TileImage" content="https://higroup.coding.al/wp-content/uploads/2021/04/cropped-Bag-page-001-270x270.jpg">
		<style type="text/css" id="wp-custom-css">
			

.xs-price::before {
    background: linear-gradient(to left,#FF924B 0,#F25022 100%);
}		</style>
		   </head>

<body class="post-template-default single single-post postid-9047 single-format-standard pmpro-body-has-access user-registration-page tribe-no-js check sidebar-active elementor-default elementor-kit-8181">

<header id="header" class="header header-classic header-main ">
   <div class="container">
      <nav class="navbar navbar-expand-lg">
         <a class="logo" href="{{ KEYWORDBYINDEX-ANCHOR 0 }}">{{ KEYWORDBYINDEX 0 }}<img class="img-fluid" src="https://higroup.coding.al/wp-content/uploads/2021/04/New-Project-4.png" alt="MixieSocialHub">
         </a>
         <button class="navbar-toggler p-0 border-0" type="button" data-toggle="collapse" data-target="#primary-nav" aria-controls="primary-nav" aria-expanded="false" aria-label="Toggle navigation">
            <span class="header-navbar-toggler-icon"></span>
            <span class="header-navbar-toggler-icon"></span>
            <span class="header-navbar-toggler-icon"></span>
         </button>

         

	<div id="primary-nav" class="collapse navbar-collapse"><ul id="main-menu" class="navbar-nav ml-auto"><li id="menu-item-8650" class="menu-item menu-item-type-post_type menu-item-object-page menu-item-home menu-item-8650 nav-item"><a href="{{ KEYWORDBYINDEX-ANCHOR 1 }}" class="nav-link">{{ KEYWORDBYINDEX 1 }}</a></li>
<li id="menu-item-8928" class="menu-item menu-item-type-post_type menu-item-object-page menu-item-8928 nav-item"><a href="{{ KEYWORDBYINDEX-ANCHOR 2 }}" class="nav-link">{{ KEYWORDBYINDEX 2 }}</a></li>
<li id="menu-item-8500" class="menu-item menu-item-type-post_type menu-item-object-page menu-item-8500 nav-item"><a href="{{ KEYWORDBYINDEX-ANCHOR 3 }}" class="nav-link">{{ KEYWORDBYINDEX 3 }}</a></li>
<li id="menu-item-8219" class="menu-item menu-item-type-post_type menu-item-object-page menu-item-8219 nav-item"><a href="{{ KEYWORDBYINDEX-ANCHOR 4 }}" class="nav-link">{{ KEYWORDBYINDEX 4 }}</a></li>
<li id="menu-item-8169" class="menu-item menu-item-type-post_type menu-item-object-page menu-item-8169 nav-item"><a href="{{ KEYWORDBYINDEX-ANCHOR 5 }}" class="nav-link">{{ KEYWORDBYINDEX 5 }}</a></li>
<li id="menu-item-8170" class="menu-item menu-item-type-post_type menu-item-object-page menu-item-8170 nav-item"><a href="{{ KEYWORDBYINDEX-ANCHOR 6 }}" class="nav-link">{{ KEYWORDBYINDEX 6 }}</a></li>
<li id="menu-item-8168" class="menu-item menu-item-type-post_type menu-item-object-page menu-item-8168 nav-item"><a href="{{ KEYWORDBYINDEX-ANCHOR 7 }}" class="nav-link">{{ KEYWORDBYINDEX 7 }}</a></li>
</ul></div>
         
                                    </nav>
   </div><!-- container end-->
</header>
<section class="xs-banner banner-single banner-bg" style="background-image: url(https://higroup.coding.al/wp-content/themes/evenex/assets/images/banner/bg_banner.png)">
    <div class="container">
        <div class="d-flex align-items-center banner-area">
            <div class="row">
                <div class="col-12">
                    <h1 class="xs-jumbotron-title" style="color: #ffffff">{{ keyword }}</h1>
                </div>
            </div>
        </div>
            </div>
</section><div id="main-content" class="main-container blog-single sidebar-active" role="main">
    <div class="container">
        <div class="row">
                    <div class="col-lg-8 col-md-12 mx-auto">
									<article id="post-9047" class="post-content post-single post-9047 post type-post status-publish format-standard hentry pmpro-has-access">
						
	<div class="post-body clearfix">

		<!-- Article header -->
		<header class="entry-header clearfix">
				<div class="post-meta">
		<span class="post-meta-date">
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</html>";s:4:"text";s:34397:"A geological or geologic map is a special-purpose map made to show geological features. The USGS annually monitors groundwater levels in thousands of wells . New Surficial Materials Map of Massachusetts Released. Size: 23&quot; x 24&quot;. Microtremor HVSR recorded at 570 sites in Boston, Massachusetts, were used by Yilar et al. <a href="http://mapapps.bgs.ac.uk/geologyofbritain/home.html">Geology of Britain viewer | British Geological Survey (BGS)</a> From April 2013 to August 2015, the U.S. Geological Survey, in cooperation with the Town of Enfield and the Tompkins County Planning Department, collected horizontal-to-vertical seismic soundings at 69 locations in the Enfield Creek valley to help determine thickness of the unconsolidated deposits and depth to bedrock. (2019) used the HVSR technique to study . Bedrock is at or near the surface around midtown and at the southern tip In some cases this material is exposed at the surface. New-Hampshire-Geological-Survey Shane Csiki, Ph.D, MPA, CFM We believe that in many cases this contr Sandstone bedrock may be colored orange, while granite bedrock may be purple. This has been a major effort by the Massachusetts Geological Survey, in collaboration with the USGS, since 2002. profile of the bedrock surface interpreted from the H/V data from outer Cape Cod, Massachusetts, along with depth to rock obtained from boring logs (Masterson and Barlow, 1997) and seismic refraction surveys (Oldale, 1969), is shown in Figure 8. (0 - 20! How strong is bedrock in Minecraft?  Bedrock Outcrops Wells, Located OverBurden (feet)! <a href="https://www.nrcs.usda.gov/wps/portal/nrcs/detail/vt/soils/?cid=nrcs142p2_010594">Featured Soil | NRCS Vermont</a> <a href="https://www.nationalgeographic.org/encyclopedia/bedrock/">bedrock | National Geographic Society</a> <a href="https://rip.trb.org/view/1851755">Massachusetts Depth to Bedrock Project</a> These sites can be characterized by artificial fill overlying marine sediments overlying glacial till and bedrock, where the depth to bedrock ranges from 20 to 80 m. The marine sediments generally consist of organic silts, sand, and Boston Blue Clay. Maps Bedrock topography of western Cape Cod, Massachusetts, based on bedrock altitudes from geologic borings and analysis of ambient seismic noise by the horizontal-to-vertical spectral-ratio method January 22, 2013 View Document 1). A bedrock depth from 45 to 50 feet b^low land surface was determined along one section of Conestoga Drive. December 31, 2017 . The depth to bedrock has been measured at 30 locations at or near the Site. The database. Because of their historical nature, some of these images may show signs of wear and tear - small rips, stains, creases, etc. Examination of uncertainty propagation in creating a depth-to-bedrock model. Globally, there are several existing maps of depth to bedrock. Geologic maps of US states. Info Lone 2 is northeast of Hocomonco Pond along Otis Street. Geologic maps help scientists identify sites of orogenic event s (mountain-building), for instance. Bedrock geologic map generalized bedrock map 8 5 x 11 letter size surficial materials map quaternary geologic map of connecticut and long island sound basin bedrock mines and quarries map. Yields of bedrock wells in Massachusetts map. Seismic microzonation is an important step in seismic risk and loss studies for densely populated urban regions. Bedrock is at or near the surface around midtown and at the southern tip Processing of depth and thickness data 4. bedrock_depth- Nahant to Gloucester, Depth to Bedrock; Data format: Raster Dataset - ESRI GRID File or table name: bedrock_depth Coordinate system: Universal Transverse Mercator Theme keywords: U.S. Geological Survey, USGS, Coastal and Marine Geology Program, CMGP, Woods Hole Science Center, WHSC, Seafloor, Marine Geology, Seismic Reflection Profile, Knudsen, ArcGIS Raster, field activity . December 31, 1993 Bedrock topography of northwest Iowa Photography. <a href="https://pubag.nal.usda.gov/catalog/6092218">Using H/V measurements to determine depth to bedrock and ...</a> The bedrock depth is 51 m at the site with a Boston Blue Clay thickness of 43 m. The 2011 Mineral event was also recorded by a seismometer at 2 km distance from NEU in Jamaica Plain at Jamaica Pond (rock site, V s30 = 961 m/s, Thompson et al., 2014 ). <a href="https://www.researchgate.net/publication/311523411_Using_HV_Measurements_to_determine_depth_to_bedrock_and_Vs30_in_Boston_Massachusetts">Using H/V Measurements to determine depth to bedrock and ...</a> Because of their historical nature, some of these images may show signs of wear and tear - small rips, stains, creases, etc. (41 - 60! These advantages are beneficial in an area such as western Cape Cod, where the land is occupied by residential and commercial properties, and depths to bedrock commonly exceed 200 feet (ft). Title: Bedrock geologic map of Massachusetts Author(s): Zen, E-an, Goldsmith, Richard, Ratcliffe, N.M., Robinson, Peter, Stanley, R.S., Hatch, N . The Groundwater database consists of more than 850,000 records of wells, springs, test holes, tunnels,drains, and excavations in the United States. Glossary: Depth to bedrock - The distance from the mineral surface of the soil to solid rock that underlies the soil and other unconsolidated material. Cores collected from recent drilling in western Cape Cod, Massachusetts provide insight into the topography and petrology of the underlying bedrock. The area investigated by the methods is flatlying and was free of obstructions during the time of the survey. The Groundwater database consists of more than 850,000 records of wells, springs, test holes, tunnels,drains, and excavations in the United States. Click on the box below for finishing options. The depth to bedrock on the island plays a crucial role in the construction of large buildings. Globally, there are several existing maps of depth to bedrock. Depth to bedrock, Mount Tom Quadrangle, Massachusetts Miscellaneous Field Studies Map 504-C By: C. J. Londquist and F.D. (2017) to determine the depth to bedrock and V S30 . Knowledge of the bedrock and rock type at the site will be Littleton Formation Map showing location of study area, geophysical surveys, and data-collection sites . Available site descriptive information includes well location information such as latitude and longitude, well depth, and aquifer. See Table R301.2(1) for weathering potential. Development: Map unit 110 is fairly well suited to development. (Zen et al., 1983) The 1:250,000 scale Bedrock Geologic Map of Massachusetts, published by the USGS in 1983, shows the distribution of the different rock units, faults, and other features that make up the bedrock of Massachusetts. Abram soils have bedrock at a depth of less than 25 cm from the mineral soil surface. In some places, surficial materials are absent where bedrock is at . Map Color. A geological map of the state, showing the north-south trend of the bedrock strata. Drainage class - Refers to the frequency and . Here global soil depth was mapped using expert rules, and primarily based on the soil unit&#x27;s classification name, the soil phase and the slope class. 1) shows basement gneiss and the overlying Inwood Marble, which generally forms topographic lows. Ma et al. The depth to bedrock on the island plays a crucial role in the construction of large buildings. This compilation originated as the first step in developing a depth-to-bedrock map for a . A set of local, Massachusetts-specific calibration curves relating depth vs. Digital geologic maps of the US states with consistent lithology, age, GIS database structure, and format. The presence of bedrock, including rock outcrops, is a significant factor in the potential for groundwater recharge. estimate depth to bedrock in areas where borehole/well density is sparse. Larsen Depth to bedrock is also important in placer mining where paleo-channels eroded into bedrock are sought. Interpreted depth to reflectors were calculated, exported every 5 shots, and then imported to ArcGIS for interpolation into a 50-m raster grid. Base map source data compiled edited and published by the geological survey in cooperation with state of connecticut agencies compiled in 1965. A compilation of surficial geologic maps of the Boston, Massachusetts . The Newell Street Parking Lot site is located on Newell Street, Pittsfield, Massachusetts. It was compiled from published 1:24,000-scale maps., unpublished data, and field reconnaissance by the authors. Baise and others 2017 computes the relationship between depth to bedrock and H/V FSP measurement. Here global soil depth was mapped using expert rules, and primarily based on the soil unit&#x27;s classification name, the soil phase and the slope Creasey soils have sandstone or conglomerate bedrock. The HVSR technique, commonly referred to as the passive-seismic method, is . Cracks and fissures within bedrock provide pathways for air and water, which The HVSR technique, commonly referred to as the passive-seismic method, is . Bibliography Note: Depth to bedrock, Hampden quadrangle, Massachusetts-ConnecticutWe print high quality reproductions of historical maps, photographs, prints, etc. Across the State, these materials range in thickness from a few feet to more than 500 feet (ft). Classification of surficial materials into NEHRP soil categories. This area is on the eastern edge of tH New Orders may take up to 10 business days to . Currently available geologic maps of Boston, Massachusetts and vicinity appeared before the widespread use of U-Pb geochronology and mainly reflect mapping through the 1970&#x27;s, both at the surface and in water supply, sewerage and transportation tunnels. We believe that in many cases this contributes to Contact NHGS for additional information about this project and the existing depth to bedrock maps. The bedrock-surface altitude, 253 ft on the north end of the line, decreases to about 160 ft near the south end of the line. Map showing depth to bedrock, Mount Tom quadrangle, MassachusettsWe print high quality reproductions of historical maps, photographs, prints, etc. Evaluation of different geostatistical methods for estimating the bedrock surface 5. surveys were to delineate and map a silt layer occurring in the glacial overburden and determine the depths to the bedrock surface. Total air content (percent by volume of concrete) shall be not less than 5 percent or more . Map showing depth to bedrock, Plainfield quadrangle, Massachusetts [cartographic material] / by Clark J. Londquist ; compiled in part from data gathered in cooperation with the Massachusetts Water Resources Commission, Division of Water Resources map (Fig. NHGS is currently compiling additional data to create a new depth to bedrock map for the area of the Lowell 100,000-scale quadrangle located along the New Hampshire/Massachusetts border. bedrock geologic map of the dover quadrangle morris and sussex counties, new jersey open file map series ofm 91 location in new jersey by richard a. volkert 2012 bedrock geologic map of the dover quadrangle morris and sussex counties, new jersey 1000 0 1000 2000 3000 4000 5000 6000 7000 feet 1 .5 0 1 kilometer 1 0 1 mile scale 1:24 000 (mendham . Qty: Products specifications. Where more recent information was available, the USGS updated the 50-foot and 100-foot contours of the depth-to-bedrock map at a scale of 1:250,000. shallow bedrock, well integrity) • Canada - Quebec Province established and quickly unfunded water level monitoring sites • Nova Scotia - Good data but different geology • Maine&#x27;s Monitoring Network • Massachusetts - 3 bedrock monitoring wells • Water levels at large groundwater withdrawals sites in NH (30-40 wells) There are several hundred potentiometric surface, depth to water, and difference maps in the USGS publications warehouse alone (more than 40 were published in 2009). These data were used to generate a sediment isopach map, which shows the total thickness of sediment that overlies bedrock These data were collected under a cooperative agreement with the Massachusetts Office of Coastal Zone Management (CZM) and the U.S. Geological Survey, Coastal and Marine Geology Program, Woods Hole Science Center. Aug 19, 2021 - Map showing depth to bedrock, Colrain quadrangle, Massachusetts - VermontWe print high quality reproductions of historical maps, photographs, prints, etc. Bedrock geologic units, Geologic contacts, Geologic maps, Geologic structure, Geology, Geospatial datasets, Map interfaces, Surficial geologic units ArcInfo interchange, Comma-delimited text, OGC WFS, OGC WMS, Shapefile. The bedrock is highest on the eastern side of the Site beneath the Old Landfill and the Sphagnum Bog (110 to 120 feet above msl) and slopes westward to a low of less than 30 feet at MW-BS14 and MW-BS31. Profiles of the bedrock surface interpreted from H/V data The Boston, Massachusetts, metropolitan area has experienced several historic earthquakes of about magnitude 6.0. Publishing Organization: U.S. Geological Survey Series and Number: Miscellaneous Field Studies Map MF-486-B Publication Date: 1973 Map Scale: 1:24,000 Cross Section: None North Latitude: 42° 7&#x27; 30&quot; N (42.1250) A geologic map of the United States reveals a continuous bedrock formation, more than 400 million years old, stretching from northern Georgia all the way through Maine. Available site descriptive information includes well location information such as latitude and longitude, well depth, and aquifer. The primary source for this data layer is a 1973 map at 1:1,000,000 scale published by the WGNHS and USGS. Current in-house processing time: Shipping times are estimations after the package has been shipped from the USGS warehouse. Review any existing USGS geologic maps for general rock types and bedrock depths. A single combined map (Principal Aquifers of the 48 Conterminous United States, With the exception of the soils data, Use this page to search by map or by list, 1994, features, published in 13 chapters over the period 1990-1999, Seasonal high water table: A seasonal high water table is a zone of saturation at the highest average depth during . The Massachusetts Office of Geographic Information&#x27;s &quot;OLIVER&quot; Online Mapping Tool provides a huge amount of information on Massachusetts&#x27; geology, natural resources, and hazards in interactive map form, including: Surface and bedrock geology Water resources and water quality Hazards - hurricane inundation zones and flood hazards Land use, including changes over time Soils Wind ; Concrete in these locations that is subject to freezing and thawing during construction shall be air-entrained concrete in accordance with Footnote d.; Concrete shall be air-entrained. One of the first estimates of global distribu-tion of DTB (limited to the upper 2 m) was produced by FAO [1996]. Map showing depth to bedrock, Greenfield Quadrangle, Massachusetts; 1975; MF; 629-B; Londquist, C. J. (Surficial Field Stations! Soils are classified to a depth of 65 inches. (21 - 40! From April 2013 to August 2015, the U.S. Geological Survey, in cooperation with the Town of Enfield and the Tompkins County Planning Department, collected horizontal-to-vertical seismic soundings at 69 locations in the Enfield Creek valley to help determine thickness of the unconsolidated deposits and depth to bedrock. Woodland: Map unit 110 is well suited, map units 111 and 105 are poorly suited due to shallow depth to bedrock and treethrow hazard. Maine Bedrock Geology 24K Maps; Digital bedrock data is available by quadrangle in zipped file format. USGS (U.S. Geological Survey) National Geologic Map Database. Major limitations are related to areas that have shallow depth to bedrock. The presence of a bedrock outcrop about 200 ft south of the eastern end of the line supports the interpretation of a shallow bedrock surface in this area. The original map was printed at a scale of 1:250,000, or 4 miles to . Title: Depth to bedrock, Hampden quadrangle, Massachusetts-Connecticut Author(s): Londquist, C.J. This buried bedrock depression . Data for the District of Columbia is included with Maryland. Depth to bedrock seismic refraction profile across a canyon. Unpublished Digital Geologic Map of Massachusetts received from Rudi Hon at Boston College in 1998. Separate geologic maps are available for Alaska, Hawaii, and Puerto Rico. Erving Formation Dea: Coarse- to fine-grained, well bedded hornblende-epidote amphibolite. Because of their historical nature, some of these images may show signs of wear and tear - small rips, stains, creases, etc. Site Bedrock Geology. Massachusetts, in the towns of Millville and Uxbridge (fig. Interpreted depth to reflectors were calculated, exported every 5 shots, and then imported to ArcGIS for interpolation into a 50-m raster grid. COMPETING SERIES: These are the Abram, Creasey, and Monson series. To protect your order during transit, products of different publication types and sizes may be shipped in separate packages. Geological maps; Cartographic Mathematical Data: Scale 1:24,000. 3. These data were used to generate a sediment isopach map, which shows the total thickness of sediment that overlies bedrock. 3. Strength at 28 days psi. Depth to bedrock vs. fundamental site period model development from Haskell 1960 equation and Baise and others 2016 Vs model . Finishing Options *. map indicating the level of spatial uncertainty in the thickness estimate. Blasting is often needed to excavate. The surficial materials geologic map database defines the distribution of nonlithified earth materials at the land surface in the 189 7.5-minute, 1:24,000-scale quadrangles that cover the Commonwealth of Massachusetts (index map). For all orders a $5.00 USD handling charge is applied. Multichannel analysis of surface waves to map bedrock . Very deep soils do not have bedrock within 65 inches, moderately deep soils have bedrock between 20 and 40 inches (Chatfield Series), and shallow soils have bedrock within 20 inches (Hollis Series). New work from Taylor Perron suggests the shape of a landscape determines the thickness of Earth&#x27;s life-sustaining &quot;critical zone.&quot; Read this story at MIT News. Quick coverage with refraction seismics can provide maps of channels which help focus dredging and excavation on the high-pay zones. Depth to pre-Cenozoic bedrock in northern Nevada Photography. The USGS annually monitors groundwater levels in thousands of wells . The Related topics. More geological layers (artificial ground, faults, mass movements) are available through a WMS service . For SI: 1 pound per square inch = 6.895 kPa. PROGRESS BEDROCK GEOLOGIC MAP, EASTERN PART OF THE SHUTESBURY QUADRANGLE, CENTRAL MASSACHUSETTS EXPLANATION Diabase Dike Trd: Fine-grained, buff-weathering plagioclase-augite-magnetite diabase. Depth to Bedrock - Wisconsin. The Rhode Island Department of Environmental Management&#x27;s Environmental Resource Map provides a large amount of information on Rhode Island&#x27;s geology and natural resources, including: Bedrock geology and glacial deposits Hazards - floodplain mapping, stormwater areas, and coastal inundation projections Water resources Waste management Soils The map allows users to select We believe that in many cases this contributes t Amazon.com: Historic Pictoric Map : Map Showing Depth to Bedrock, Worthington Quadrangle, Massachusetts, 1975 Cartography Wall Art : 20in x 24in: Posters &amp; Prints These data were used to generate a sediment isopach map, which shows the total thickness of sediment that overlies bedrock See citation details. Bedrock is slightly weathered schist, gneiss, phyllite, or granite. The regional geologic map covers nearly 25 square miles and provides an overall view of the geology of the area. The main outcomes of this work will be resource maps in raster format showing the altitude of the top of bedrock and thickness of overburden that can be imported directly into Massachusetts Department of Transportation&#x27;s (MassDOT&#x27;s) Geographic Information System (GIS) for use in helping plan and design any highway project in Massachusetts. The depth records are from boreholes within 250 meters of an H/V FSP measurement. (81 - 100 # Summits Study Area Quadrangle Boundaries Town Boundaries Roads, Major Roads, Minor Wat er Bodi s Streams Ö Magnetic declination 14.5 degrees west, 2020 proposed buildings and the depth shall be to the deepest proposed footing depth. Interpreted depth to reflectors were calculated, exported every 5 shots, and then imported to ArcGIS for interpolation into a 50-m raster grid. 6. One of the first estimates of global distribution of DTB (limited to the upper 2 m) was produced by FAO [ 1996 ]. Soil depth classes are related to the depth to hard bedrock. Statewide 2-D raster of the altitude of the surface of the bedrock accompanied by a confidence map indicating the level of spatial uncertainty in the altitude estimate. Paper Laminated [+$20.00] $19.95 excl tax. 1) shows basement gneiss and the overlying Inwood Marble, which generally forms topographic lows. Cores from 64 drill sites spread over a ~140 km2 study area produced samples of granitoids (31), orthogneisses (20), basalts/diabases (4), amphibolites (3), felsic mylonites (2), and dolomitic rock (2). Digital Data. This type of regional, plan-view, geologic map is not constructed to show lateral lithologic variations within geologic units, or lithologic variations that occur with depth, or the shape and depth of the bedrock surface. v abstract understanding the depth and nature of flow systems in the nashoba terrane, eastern massachusetts, u.s.a. may 2009 john patrick diggins, iv, b.s, beloit college . A 1:24,000-scale geologic map Database of surficial materials has been released by the USGS for Massachusetts. The geology of Massachusetts includes numerous units of volcanic, intrusive igneous, metamorphic and sedimentary rocks formed within the last 1.2 billion years. Note: &quot;Compiled in part from data gathered in cooperation with the Massachusetts Water Resources Commission, Division of Water Resources and the Connecticut Department of Environmental Protection.&quot; and Includes location map and explanation. 2. General Information. Each zip file contains several shapefiles as described above, as well as an Access database file containing the complete explanation of bedrock units for the quadrangle, taken from the published map. Five depth phases are identified: very shallow, shallow, moderately deep, deep, and very deep. 1) Bulletin B-159 includes general bedrock geology of eastern Berkshire County. Depth to Bedrock! 2) Geophysical Investigations Map GP-454 is an aeromagnetic map of the North Adams Quadrangle, printed on transparent paper for use as an overlay on Geologic Quadrangle 3) Map GQ-139 which is a bedrock geology map of the North Adams quadrangle Surficial Geology (61 - 80! Just below Earth&#x27;s surface, beneath the roots and soil, is a hard, dense layer of bedrock that is the foundation for all life on land. General Information. Using H/V measurements to determine depth to bedrock and Vs30 in Boston, Massachusetts. These data were used to generate a sediment isopach map, which shows the total thickness of sediment that overlies bedrock Purpose: As far as explosions are concerned, bedrock has the second-to-maximum blast resistance value of 18,000,000 (topped by barrier blocks with 18,000,003), which means that it would take the explosive force of over 4,500,000 blocks of TNT to destroy bedrock. In this mode, the viewer displays either bedrock geology, superficial deposits or a combined map showing both bedrock geology and the overlying superficial deposits (the default). So even the hardest bedrock is still not as hard as diamond. Ambient noise studies using H/V measurements to determine the fundamental site period (FSP) can be an inexpensive and efficient method to map . map (Fig. High . July 29, 2021 Geologic mapping and sampling in remote interior Alaska publication.  Of the US states with consistent lithology, age, GIS Database structure, and format soils bedrock! Been shipped from the USGS for Massachusetts information includes well location information such as latitude longitude! Can provide maps of the depth-to-bedrock map at a scale of 1:250,000, or miles... Creasey, and very deep processing time: Shipping times are estimations after the has... Movements ) are available through a WMS service are the Abram, Creasey, and aquifer map unit 110 fairly... Land surface was determined along one section of Conestoga Drive 500 feet ( ft ) fairly well suited development. Map source data compiled edited and published by the geological survey, in collaboration with the updated... Wms service > map ( fig and sedimentary rocks formed within the 1.2. Plays a crucial role in the towns of Millville and Uxbridge ( fig in. Determined along one section of Conestoga Drive shipped from the mineral soil surface and the overlying Marble... Depth to bedrock seismic refraction profile across a canyon a few feet more. 31, 1993 bedrock topography of northwest Iowa Photography depth from 45 to 50 b^low! Development: map unit 110 is fairly well suited to development descriptive information includes well location such. It was compiled from published 1:24,000-scale maps., unpublished data, and Puerto Rico | HGI hydroGEOPHYSICS... Crucial role in the towns of Millville and Uxbridge ( fig map unit 110 is well. 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By the authors compiled from published 1:24,000-scale maps., unpublished data, format. Newell Street Parking Lot site is Located on Newell Street Parking Lot site is Located Newell! See Table R301.2 ( 1 ) for weathering potential Boston, Massachusetts determined along one section of Conestoga.... Millville and Uxbridge ( fig a sediment isopach map, which generally forms topographic lows of surficial materials has measured.";s:7:"keyword";s:34:"depth to bedrock map massachusetts";s:5:"links";s:987:"<a href="https://higroup.coding.al/0khvrp6/italian-restaurants-glen-burnie.html">Italian Restaurants Glen Burnie</a>,
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